Egina Deep Water Development: Isolation Barrier Valve Case Study

2018 ◽  
Author(s):  
G. Forrest ◽  
C. Morand ◽  
K. Johnson ◽  
V. Okengwu ◽  
V. Chaloupka
Keyword(s):  
Deep Water ◽  
Water Development

Review of sand control results and performance on a deep water development - A case study from the Girassol Field, Angola

2004 ◽  
Author(s):  
Eric Delattre ◽  
Jean François Authier ◽  
François Rodot ◽  
Gerard Petit ◽  
Jacques Alfenore
Keyword(s):  
Deep Water ◽  
Water Development ◽  
Sand Control ◽  
And Performance

Egina Deep Water Development: Isolation Barrier Valve Case Study

2019 ◽  
Author(s):  
C. Okpalla ◽  
V. Chaloupka ◽  
V. Okengwu ◽  
M. MacMillan ◽  
D. Ezugworie ◽  
...  
Keyword(s):  
Deep Water ◽  
Water Development

scholarly journals Stratigraphic and tectonic control of deep-water scarp accumulation in Paleogene synorogenic basins: a case study of the Súľov Conglomerates (Middle Váh Valley, Western Carpathians)

2017 ◽  
Vol 68 (5) ◽  
pp. 403-418 ◽  
Author(s):  
Ján Soták ◽  
Zuzana Pulišová ◽  
Dušan Plašienka ◽  
Viera Šimonová
Keyword(s):  
Deep Water ◽  
Fault Scarp ◽  
Submarine Landslides ◽  
Orogenic Wedge ◽  
Calcite Veins ◽  
Tectonic Erosion ◽  
Mass Flow Deposits ◽  
Miocene Tectonics ◽  
Mass Transport Deposits

Abstract The Súľov Conglomerates represent mass-transport deposits of the Súľov-Domaniža Basin. Their lithosomes are intercalated by claystones of late Thanetian (Zones P3 - P4), early Ypresian (Zones P5 - E2) and late Ypresian to early Lutetian (Zones E5 - E9) age. Claystone interbeds contain rich planktonic and agglutinated microfauna, implying deep-water environments of gravity-flow deposition. The basin was supplied by continental margin deposystems, and filled with submarine landslides, fault-scarp breccias, base-of-slope aprons, debris-flow lobes and distal fans of debrite and turbidite deposits. Synsedimentary tectonics of the Súľov-Domaniža Basin started in the late Thanetian - early Ypresian by normal faulting and disintegration of the orogenic wedge margin. Fault-related fissures were filled by carbonate bedrock breccias and banded crystalline calcite veins (onyxites). The subsidence accelerated during the Ypresian and early Lutetian by gravitational collapse and subcrustal tectonic erosion of the CWC plate. The basin subsided to lower bathyal up to abyssal depth along with downslope accumulation of mass-flow deposits. Tectonic inversion of the basin resulted from the Oligocene - early Miocene transpression (σ1 rotated from NW-SE to NNW-SSE), which changed to a transpressional regime during the Middle Miocene (σ1 rotated from NNE-SSW to NE-SW). Late Miocene tectonics were dominated by an extensional regime with σ3 axis in NNW-SSE orientation.

Integrated Reservoir Petrophysical Characterization and 3D Modeling: a Deep-Water Turbidite Reservoir Case Study

2008 ◽  
Author(s):  
Livio Ruvo ◽  
Mirko Calderoni ◽  
Marco Cesaro ◽  
Franco Fonnesu ◽  
Ilario Franco ◽  
...  
Keyword(s):  
Deep Water ◽  
3D Modeling

scholarly journals Constraining sub-seismic deep-water stratal elements with electrofacies analysis; A case study from the Upper Cretaceous of the Måløy Slope, offshore Norway

2015 ◽  
Vol 59 ◽  
pp. 268-285 ◽  
Author(s):  
Amandine Prélat ◽  
David M. Hodgson ◽  
Mark Hall ◽  
Christopher A.-L. Jackson ◽  
Carol Baunack ◽  
...  
Keyword(s):  
Deep Water ◽  
Upper Cretaceous

Probable Causes for the 1972 Red Tide in the Cape Ann Region of the Gulf of Maine

1973 ◽  
Vol 30 (9) ◽  
pp. 1363-1366 ◽  
Author(s):  
Hugh Francis Mulligan
Keyword(s):  
Deep Water ◽  
Heavy Rainfall ◽  
Gulf Of Maine ◽  
Red Tide ◽  
Hydrographic Data ◽  
Water Development ◽  
Seed Population ◽  
Causative Factors ◽  
Vertical Distributions

Hydrographic data and spatial, temporal, and vertical distributions of Gonyaulax tamarensis are presented from the vicinity of Cape Ann, Massachusetts in summer of 1972. When considered together with available meteorological records, these data provide information on probable causes and development of the September 1972 red tide bloom in the Gulf of Maine. An upwelling of deep water, development of a "seed" population of G. tamarensis during unusually dry weather in August, and heavy rainfall in September are suggested as the three causative factors.

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